Numerical Classification of Oak Forests on Loess in Hungary, Croatia and Serbia

Preslia 86: 47–66, 2014 47 Numerical classification of oak forests on loess in Hungary, Croatia and Serbia Numerická klasifikace doubrav na sprašových půdách v Maďarsku, Chorvatsku a Srbsku Dragica P u r g e r1,2, Attila L e ngyel3, Balázs K e v e y2, Gábor L e n d v a i4 András H o r v á t h3, Zagorka To m i ć5 & János C s i k y2 1National Institute for the Environment, H-7623 Pécs, Köztársaság tér 7, Hungary, e-mail: [email protected]; 2University of Pécs, Faculty of Science, Institute of Biology, Department of Plant Taxonomy and Geobotany, H-7624 Pécs, Ifjúság u. 6, Hungary, e-mail: [email protected], [email protected]; 3MTA Centre for Ecological Research, Insti- tute of Ecology and Botany, H-2163 Vácrátót, Alkotmány utca 2-4., Hungary. e-mail: [email protected], [email protected]; 4H-7000 Sárbogárd, Ady Endre út 162, Hungary, e-mail: [email protected]; 5Dr. Aleksandra Kostića 4, 11000 Belgrade, Serbia Purger D., Lengyel A., Kevey B., Lendvai G., Horváth A., Tomić Z. & Csiky J. (2014): Numerical classification of oak forests on loess in Hungary, Croatia and Serbia. – Preslia 86: 47–66. Oak forests on loess are floristically one of the richest types of broadleaved forests and are among the most threatened types of natural habitats in the Carpathian Basin. They are classified in several communities in Hungary, Croatia and Serbia. These syntaxa are distinguished mostly on the basis of traditional phytosociological methods without comparison across a larger geographical scale. The recognition of some of these local syntaxa in the field, therefore, can be difficult, and the application of their names to communities in other areas may be questionable. The goal of this study was to develop an international typology for oak forests on loess based on a numerical analysis. A data set of 437 phytosociological relevés (stands of 12 associations from three countries) was stratified and 270 relevés were analysed using multivariate statistical methods. Six types were distinguished: Primula vulgaris type (xero-mesic to mesic sub-Mediterranean closed-canopy oak forests); Ruscus aculeatus type (xeric to xero-mesic sub-Mediterranean type); Vinca herbacea type (xeric continental open-canopy woodlands); Pulmonaria mollis type (xeric to mesic continental closed-canopy forests); Corydalis cava type (mesic closed-canopy oak forests in nutrient-rich habitats); and Stellaria media type (xeric to mesic oak forests in nutrient-rich habitats). The vegetation types identified are related to syntaxa traditionally recognized by phytosociologists. Our analysis did not support the distinction of some associations with local distributions. The geographical distributions of the two main forest types exhibited a gradient-like pattern in a north-east–south-west direction. The dry continental forest steppe woodland is mainly distributed in the north-eastern part of Hungary, whereas the xero-mesic sub-Mediterranean forests are restricted to the southwestern and southern part of our study area. This pattern corresponds to a climatic gradient from the North Hungarian Mts to north-eastern Croatia and northern Serbia. Keywords:Aceri tatarici-Quercion, Carpathian Basin, forest steppe, gradient, phytosociology Introduction Loess covers large areas in the Carpathian Basin (Niklfeld 1973–1974). Despite this, oak forests on loess are restricted mainly to the transitional zone between lowlands and hilly regions and the foothills of the mountains (Zólyomi 1989, Fekete et al. 2011). These forests grow on chernozem-like soils, which are highly fertile. Palaeoecological data indicate 48 Preslia 86: 47–66, 2014 the persistent dominance of temperate deciduous wooded steppe with a varying canopy composition on the Great Hungarian Plain throughout the Holocene (Magyari et al. 2010). Changes in vegetation linked to human intervention (e.g. burning) in the landscape, expan- sion of weeds and reduction in the arboreal vegetation in the forest-steppe environment are traceable to the Late Neolithic and Early Copper Age (Sümegi et al. 2012). The loss of tree cover during the last two millennia is almost certainly a result of intense agricultural exploitation of the area (Magyari et al. 2010). These forests survived only as fragments, of which many were subject to strong anthropogenic influences (Zólyomi 1957, 1958, Molnár et al. 2000). Stands of these forests may differ substantially due to human manage- ment, local conditions, as well as variation in climate and altitude. Tree growth and cover range from small trees and scattered groups of trees on the driest or most disturbed sites to well-developed forests with closed canopy on more favourable sites. There is an extremely high risk that there will be a decline in the floristic richness of the small isolated fragments of forests, especially those at the limits of their geographical range. According to Borhidi & Sánta (1999), species-rich loess oak forests are relicts and worthy of strict protection. In Annex I of the Habitat Directive, these types of forest are designated with the code: 91I0 Euro-Siberian steppe woodlands and forests with Quercus spp. and indicated as a priority habitat (http://ec.europa.eu/environment/nature/legislation/habitatsdirective). Continental xero-thermophilous oak forests in the central and eastern part of Europe were surveyed and first synthesized by Zólyomi (1957, 1958). The communities described were included in the alliance Aceri tatarici-Quercion Zólyomi & Jakucs 1957. The southern limit of the distribution of loess oak forests runs across south-western Hungary, north- eastern Croatia and the northern part of Serbia (Horvat et al. 1974, Jakucs 1974, Jovanović 1997). However, there is no unified syntaxonomy of this vegetation type, which hinders cross-border communication. North-eastern Croatia is a part of the Pannonian Plain (Horvat 1954, Ilijanić 1966). The potential vegetation of this transitional forest steppe zone is oak forest on loess belonging to the Carpinion betuli alliance (Rauš 1971, 1976). Small fragments of oak forest also occur on the loess plateau on the Bansko hill (Purger & Csiky 2008). These stands are unique in Croatia as some rare continental species occur in them, but their syntaxonomical status is unclear. In northern Serbia (Vojvodina province), the oak forests on loess described by Slavnić (1952) are included in the Carpinion betuli alliance (Jovanović et al. 1986a, b). However, the potential natural vegetation of the loess plateau is considered to be a mosaic of forest steppe vegetation belonging to the alliance Aceri tatarici-Quercion (Parabućski & Janković 1978, Jovanović 1997). Nevertheless, delimitation of the oak forests on loess assigned to different alliances is not clear. There is a continuous transition within xeric and mesic forest types, in which the composition of the herb layer varies considerably depending on soil moisture, nutrient availability and openness of the canopy (Kevey 2008). Several different associations of oak forests on loess occur in Hungary, Croatia and Serbia (Table 1). These syntaxa with restricted distributions are distinguished mostly on the basis of traditional phytosociological methods without comparing them with others at a larger geographical scale and thus it is difficult to recognize them in nature. To clarify the syntaxonomical relationships of the communities described, we carried out a classification of forests growing on loess in the three countries. Our objectives were to answer the following questions by using a large international geographically stratified data set: (i) What types of loess oak forest can be distinguished in the study area using multivariate Purger et al.: Numerical classification of oak forests 49 statistical analyses? (ii) What are the differences between these types in terms of diagnos- tic, dominant and constant species? (iii) What are the differences between these types in terms of ecological features based on indicator values? (iv) Is there a gradient in forest vegetation in these three neighbouring countries? (v) Do the results obtained by multivariate methods correspond with those based on traditional classification? Material and methods Study area Oak forests on loess currently occur in a limited area in Hungary (Zólyomi et al. 2013): in the Gödöllő and Velence hills (Fekete 1965), the North Hungarian Mts, the Mezőföld (Borhidi et al. 2012), the Tolna hills and on the Nyárád-Harkány Plain (Kevey 2008). In Croatia, this type of vegetation occurs in the north-eastern part of the country (Rauš et al. 1985, Franjić et al. 2005) on the western slopes of the Fruška Mts (Rauš 1971), the loess plateau near Đakovo (Rauš 1976) and Bansko hill (Purger & Csiky 2008, Csiky & Purger 2013). In northern Serbia (Vojvodina province) it occurs on lowland loess terraces in the foothills of the Fruška Mts and Titel hill (Jovanović 1997). We analysed a data set from these areas (Fig. 1). The climate in the study area has a transitional character. In the eastern part of Hungary, it is moderately continental, whereas sub-Mediterranean influences are stronger towards the south and southwest. In addition, the strength of continental and sub-Mediterranean climatic influences changes from year to year (Zólyomi et al. 1997). According to the climatic maps of Hungary (Mersich et al. 2002), the range of the mean annual precipitation increases from 500–550 mm in the central part of the Great Plain to 550–600 mm towards the north-eastern part of Hungary and the Danube region, and even further to 600–700 mm in the South Transdanubian region. The range of the average annual temperature increases from 8–10 °C to 10–12 °C in the same direction. In north-eastern Croatia, the mean annual precipitation amounts to 651 mm, while the average annual temperature is 10.8 °C. This climate is warm-temperate without a drought period. Precipitation is rather evenly distributed throughout the year, with winter being the driest (Seletković & Katušin 1992). The distribution of precipitation in northern Serbia (Vojvodina province) follows a predomi- nantly continental pattern with higher amounts of rainfall in June.

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